Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4716762 | Lithos | 2011 | 15 Pages |
Abstract
⺠Gabbro-norite intrusions in Alpine -Apennine ophiolites. ⺠Parental melts were strongly depleted asthenospheric fractional melts. ⺠Melt silica saturation via melt-peridotite reaction (pyroxenes' dissolution - olivine precipitation) during porous flow percolation.
Keywords
Related Topics
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Geochemistry and Petrology
Authors
G.B. Piccardo, L. Guarnieri,